Felsőbányaite (original) (raw)
A valid IMA mineral species - grandfathered
About FelsőbányaiteHide
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Formula:
Al4(SO4)(OH)10 · 4H2O
Colour:
Colourless, yellow, white; colourless in transmitted light.
Crystal System:
Monoclinic
Name:
From the type locality, Felsöbánya, Hungary (now Baia Sprie, Romania).
A hydrated aluminium sulfate first described by Kenngott in 1853 (as felsöbányite). However, the mineral was earlier observed around 1841/42 by Haidinger in the collection of the Imperial and royal Chamber of Mining, Vienna (Papp, 2004).
Later Bannister & Hollingworth (1948) described a white compact mineral with conchoidal fracture and a white plastic clay-like appearance from Old Lodge Pit, Northamptonshire, England, UK, and gave it the name basaluminite (a BASic sulfate of ALUMINum).
Farkas & Pertlik (1997) showed that basaluminite is identical with felsőbányaite, and basaluminite was discredited by IMA in 2006 (Burke, 2006). The name felsőbányaite has priority over "basaluminite" which wasn't named until 1948.
May originate as a dehydration product of hydrobasaluminite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:1474:4
eb9f9c9d-b2bb-4589-b523-e42807a664a6
IMA Classification of FelsőbányaiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
Type description reference:
Classification of FelsőbányaiteHide
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7.DD.05
7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
D : Sulfates (selenates, etc.) with additional anions, with H2O
D : With only medium-sized cations; sheets of edge-sharing octahedra
31.4.4.1
31 : HYDRATED SULFATES CONTAINING HYDROXYL OR HALOGEN
4 : (AB)4(XO4)Zq·xH2O
25.6.8
25 : Sulphates
6 : Sulphates of Al and Tl
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Fsb | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of FelsőbányaiteHide
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Comment:
Pearly on cleavage surfaces.
Colour:
Colourless, yellow, white; colourless in transmitted light.
Cleavage:
Distinct/Good
On {010} and {100}; and possibly also on {001}.
Density:
2.33 g/cm3 (Measured) 2.20 g/cm3 (Calculated)
Optical Data of FelsőbányaiteHide
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Chemistry of FelsőbányaiteHide
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Mindat Formula:
Al4(SO4)(OH)10 · 4H2O
Crystallography of FelsőbányaiteHide
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Crystal System:
Monoclinic
Class (H-M):
2 - Sphenoidal
Cell Parameters:
a = 13.026(1) Å, b = 10.015(1) Å, c = 11.115(1) Å
β = 104.34(1)°
Ratio:
a:b:c = 1.301 : 1 : 1.11
Unit Cell V:
1,404.83 ų (Calculated from Unit Cell)
Morphology:
Occurs as globular, radial aggregates comprised of lamellar crystals; also as intergrown lath-like crystals tabular {001} and elongated [100] with a terminal angle of 66°24'.
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
9.43 Å | (>10) |
5.96 Å | (3) |
4.79 Å | (10) |
4.64 Å | (10) |
3.67 Å | (4) |
2.71 Å | (4) |
2.45 Å | (4) |
2.27 Å | (5) |
Comments:
9.43 (I/Irel = 100) not in Handbook of Mineralogy data.
Geological EnvironmentHide
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Geological Setting:
Oxide zone in marcasitic ores.
Type Occurrence of FelsőbányaiteHide
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Associated Minerals at Type Locality:
Reference:
Kenngott (1853) Königliche Akademie der Wissenschaften, Vienna, Sitzber.: 10: 294 (as Felsöbányite).
Synonyms of FelsőbányaiteHide
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Other Language Names for FelsőbányaiteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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7.DD. | Asagiite | NiCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
---|---|---|---|
7.DD.07 | Llantenesite | Cu6Al[SeO4](OH)12Cl · 3H2O | Trig. 3_m_ : P_31_c |
7.DD.10 | Langite | Cu4(SO4)(OH)6 · 2H2O | Mon. m |
7.DD.10 | Posnjakite | Cu4(SO4)(OH)6 · H2O | Mon. m : P m |
7.DD.10 | Wroewolfeite | Cu4(SO4)(OH)6 · 2H2O | Mon. m : P m |
7.DD.10 | Gobelinite | CoCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/m |
7.DD.10 | Fehrite | MgCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
7.DD.15 | Spangolite | Cu6Al(SO4)(OH)12Cl · 3H2O | Trig. 3_m_ : P_31_c |
7.DD.15 | Kobyashevite | Cu5(SO4)2(OH)6 · 4H2O | Tric. 1 : _P_1 |
7.DD.15 | Unnamed (Dimorph of Devilline) | CaCu4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _P_21/b |
7.DD.20 | Ktenasite | ZnCu4(SO4)2(OH)6 · 6H2O | Mon. 2/m : _P_21/b |
7.DD.25 | Christelite | Cu2Zn3(SO4)2(OH)6 · 4H2O | Tric. 1 : _P_1 |
7.DD.30 | Campigliaite | Mn2+Cu4(SO4)2(OH)6 · 4H2O | Mon. 2 : _B_2 |
7.DD.30 | Devilline | CaCu4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _P_21/b |
7.DD.30 | Orthoserpierite | Ca(Cu,Zn)4(SO4)2(OH)6 · 3H2O | Orth. m _m_2 : P c _a_21 |
7.DD.30 | Serpierite | Ca(Cu,Zn)4(SO4)2(OH)6 · 3H2O | Mon. 2/m : _B_2/b |
7.DD.30 | Niedermayrite | CdCu4(SO4)2(OH)6 · 4H2O | Mon. 2/m : _P_21/m |
7.DD.30 | Edwardsite | Cu3Cd2(SO4)2(OH)6 · 4H2O | Mon. 2/m : _P_21/b |
7.DD.35 | Carrboydite | (Ni1-xAlx)(SO4)x/2(OH)2 · nH2O | Hex. |
7.DD.35 | Glaucocerinite | (Zn1-xAlx)(OH)2(SO4)x/2 · nH2O | Hex. |
7.DD.35 | Honessite | (Ni1-xFe3+x)(OH)2[SO4]x/2 · nH2O | Trig. |
7.DD.35 | Hydrohonessite | (Ni1-xFe3+x)(OH)2(SO4)x/2 · nH2O | Hex. |
7.DD.35 | Motukoreaite | Mg6Al3(OH)18[Na(H2O)6][SO4]2 · 6H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Mountkeithite | [(Mg1-xFe3+x)(OH)2][SO4]x/2 · nH2O | Hex. |
7.DD.35 | Shigaite | Mn6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Trig. 3 : _R_3 |
7.DD.35 | Wermlandite | Mg7Al2(OH)18[Ca(H2O)6][SO4]2 · 6H2O | Trig. 3_m_ _(_32/m ) : _P_3_c_1 |
7.DD.35 | Woodwardite | Cu1-xAlx(OH)2(SO4)x/2 · nH2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Zincaluminite | Zn6Al6(SO4)2(OH)16 · 5H2O | |
7.DD.35 | Hydrowoodwardite | (Cu1-xAlx)(OH)2[SO4]x/2 · nH2O | Trig. 3_m_ _(_32/m ) : R_3_m |
7.DD.35 | Zincowoodwardite | Zn1-xAlx(OH)2[SO4]x/2 · nH2O | Trig. |
7.DD.35 | Natroglaucocerinite | Zn6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Hex. |
7.DD.35 | Nikischerite | Fe2+6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2O | Trig. 3 : _R_3 |
7.DD.40 | Isselite | Cu6(SO4)(OH)10 · 5H2O | Orth. m _m_2 : P m _n_21 |
7.DD.40 | Lawsonbauerite | (Mn2+,Mg)9Zn4(SO4)2(OH)22 · 8H2O | Mon. 2/m : _P_21/b |
7.DD.40 | Torreyite | (Mg,Mn2+)7◻2Mn2+2Zn4(SO4)2(OH)22 · 8H2O | Mon. 2/m : _P_21/b |
7.DD.45 | Mooreite | Mg9◻2Mn2Zn4(SO4)2(OH)26 · 8H2O | Mon. 2/m : _P_2/b |
7.DD.45 | Hodgesmithite | (Cu,Zn)6Zn(SO4)2(OH)10 · 3H2O | Trig. 3 : _P_3 |
7.DD.47 | Lahnsteinite | Zn4(SO4)(OH)6 · 3H2O | Tric. 1 : _P_1 |
7.DD.50 | Namuwite | Zn4(SO4)(OH)6 · 4H2O | Trig. 3 : _P_3 |
7.DD.50 | Minohlite | (Cu,Zn)7(SO4)2(OH)10 · 8H2O | Hex. |
7.DD.52 | Lauraniite | Cu6Cd2(SO4)2(OH)12 · 5H2O | Mon. 2/m : _P_21/b |
7.DD.55 | Bechererite | Zn7Cu(OH)13[(SiO(OH)3(SO4)] | Trig. 3 : _P_3 |
7.DD.60 | Ramsbeckite | (Cu,Zn)15(SO4)4(OH)22 · 6H2O | Mon. 2/m |
7.DD.65 | Vonbezingite | Ca6Cu3(SO4)3(OH)12 · 2H2O | Mon. 2/m : _P_21/b |
7.DD.70 | Redgillite | Cu6(SO4)(OH)10 · H2O | Mon. 2/m : _P_21/b |
7.DD.75 | Chalcoalumite | CuAl4(SO4)(OH)12 · 3H2O | Mon. 2 : _P_21 |
7.DD.75 | Nickelalumite | NiAl4(SO4)(OH)12(H2O)3 | Mon. 2/m |
7.DD.75 | Kyrgyzstanite | ZnAl4(SO4)(OH)12 · 3H2O | Mon. 2/m |
7.DD.80 | Guarinoite | Zn6(SO4)(OH)10 · 5H2O | Hex. |
7.DD.80 | Schulenbergite | (Cu,Zn)7(SO4)2(OH)10 · 3H2O | Trig. 3 |
7.DD.80 | Thérèsemagnanite | NaCo4(SO4)(OH)6Cl · 6H2O | Trig. 3 : _P_3 |
7.DD.80 | UM1992-30-SO:CCuHZn | (Zn,Cu)7(SO4,CO3)2(OH)10 · 3H2O | Trig. 3 : _P_3 |
7.DD.85 | Montetrisaite | Cu6(SO4)(OH)10 · 2H2O | Orth. m _m_2 : C m _c_21 |
Other InformationHide
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Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for FelsőbányaiteHide
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References for FelsőbányaiteHide
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Reference List:
Localities for FelsőbányaiteHide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.